Abstract
A disconformity and lag deposit that separates the Tallahatta and Lisbon Formations along Pigeon Creek near Red Level, Conecuh-Covington Counties, Alabama, contains osteichthyan remains belonging to: Pycnodus sp.; Lepisosteus sp.; Albula sp.; Egertonia sp.; Cylindracanthus rectus Agassiz, 1843; Sphyraena sp.; Trichiurides cf. T. sagittidens Winkler, 1874; Scomberomorus sp.; Aridae gen. indet.; and Ostraciidae gen. indet. This fossil osteichthyan assemblage is similar to other contemporaneous nearshore faunas found throughout Alabama, the Atlantic and Gulf Coastal Plains, and elsewhere throughout the Northern Atlantic Ocean Basin. The accumulation and concentration of osteichthyans between the Tallahatta and Lisbon Formations is the result of third order eustatic sea level fluctuation and reflects a complex taphonomic history of exhumation, transport, and reburial across a shallow, middle Eocene shelf. Wide spread distribution of osteichthyan genera found in the Pigeon Creek assemblage demonstrates the continuity of shallow marine shelf environments of the Northern Atlantic Ocean Basin during the middle Eocene and the utility of osteichthyans in regional and transatlantic stratigraphic studies.